Up: Self-similar evolution of wind-blown
4 Summary
We have investigated the evolution of a mass-loaded wind blown bubble
with a constant rate of injection of mechanical energy from a central wind
source. The mass loading occurs due to the
hydrodynamic ablation of distributed clumps, and is "switched-on'' at a
specified radius, interior to which the wind expands freely.
The requirement that the solution be self-similar imposes a link
between the radial variation of the interclump density
(
)
and the rate of mass loading from the clumps
(
)
which forces
.
We first produced solutions with negligible mass loading and
(which correspond to constant
and
),
which we compared with results obtained by Dyson (1973).
Excellent agreement for the structure of the bubble was found.
We also confirmed that for negligible mass loading, the value of
had no effect on the resulting solutions, as desired.
We then investigated the changes in the structure of the bubble for
different values of
,
,
,
and
.
The central conclusions are:
- Substantial mass loading of the wind-blown bubble can occur over
a wide range of
.
However, to additionally satisfy
the requirement that the bubble mass is larger than the mass of
the swept-up shell, low values of
are needed (e.g.
).
- The profiles of the flow variables are significantly altered under
conditions of large mass loading. With respect to solutions with negligible
mass loading, the density and temperature profiles increase, and the
velocity and Mach number profiles drop. Changes to the profiles can be
very rapid. Mass loading of the wind also reduces the Mach number prior
to the inner shock.
- The mass-loaded wind may also connect directly to the contact
discontinuity without the need for a global inner shock.
- The Mach number of the flow relative to the
clumps which are injecting the mass can take several different forms.
The flow can be either entirely supersonic, or have one (or maybe more)
sonic points.
- Whilst mass loading reduces the bubble temperature, it also
tends to reduce the emissivity in the interior of the
bubble relative to its limb, whilst simultaneously increasing the central
temperature relative to the limb temperature. The maximum temperature in
the bubble is often not the post-inner-shock temperature, but occurs near
the onset of mass loading. In some cases this can be many times greater
than the post-inner-shock temperature.
Acknowledgements
JMP would like to thank PPARC for the funding of a PDRA position, and
Sam Falle and Rob Coker for helpful discussions. We would also like
to thank an anonymous referee whose suggestions improved this paper. This
work has made use of Nasa's Astrophysics Data System Abstract Service.
Up: Self-similar evolution of wind-blown
Copyright ESO 2001